Geomagnetic Field Intensity during the Neolith in the Central East European Plain
- Autores: Nachasova I.E.1, Pilipenko O.V.1, Markov G.P.1, Gribov S.K.2, Tsetlin Y.B.3
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Afiliações:
- Schmidt Institute of Physics of the Earth
- Borok Geophysical Observatory
- Institute of Archeology
- Edição: Volume 58, Nº 3 (2018)
- Páginas: 438-447
- Seção: Article
- URL: https://journals.rcsi.science/0016-7932/article/view/156798
- DOI: https://doi.org/10.1134/S001679321803012X
- ID: 156798
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Resumo
The conducted archeomagnetic studies resulted in data on variations in the geomagnetic field intensity in the central East European Plain (Sakhtysh I site area, ϕ = 56°48′ N, λ = 40°33′ E) during the time interval of 5–3 ka BC. The geomagnetic field intensity varied mainly within the range of 30–60 μT. In the first half of the 5th millennium BC, the mean level of geomagnetic field intensity was about 35 μT. In the second half of the 5th–early 4th millennium BC, it rose to about 50 μT and then decreased again to reach a mean value of about 40 μT in the period of 4–3 ka BC. Comparison of the geomagnetic field intensity variation based on the obtained data and the data on the Caucasus region for the same time interval demonstrates a certain similarity.
Sobre autores
I. Nachasova
Schmidt Institute of Physics of the Earth
Email: pilipenko@ifz.ru
Rússia, Moscow
O. Pilipenko
Schmidt Institute of Physics of the Earth
Autor responsável pela correspondência
Email: pilipenko@ifz.ru
Rússia, Moscow
G. Markov
Schmidt Institute of Physics of the Earth
Email: pilipenko@ifz.ru
Rússia, Moscow
S. Gribov
Borok Geophysical Observatory
Email: pilipenko@ifz.ru
Rússia, Borok, Yaroslavl oblast
Yu. Tsetlin
Institute of Archeology
Email: pilipenko@ifz.ru
Rússia, Moscow
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